Summary
In the Western Dinarides the Lower Liassic carbonates are underlain by Upper Triassic “Hauptdolomit”, whereas the first appearance of the foraminiferOrbitopsella praecursor (Gümbel) marks the beginning of the Middle Liassic. Their composition, observed at several localities in Western Croatia, shows a correlation of sedimentation events, which took place during Early Liassic on the Adriatic-Dinaridic carbonate platform. Facies variability is interpreted as result of autocyclic sedimentary processes on which the carbonate platform reacted by periodical oscillations of sea-bottom near the fair-weather wavebase. As a consequence, the Lower Liassic carbonate successions in the Dinarides is characterized by stacking of two main types of coarsening-upward parasequences: (1) the basal part of the Lower Liassic succession is represented by parasequences composed of mudstones or pelletal-bioclastic wackestones as their lower members, and peloidal-bioclastic wackestone/packstones to grain-stones as their upper members; and (2) the upper part of the Lower Liassic succession with parasequences consisting of mudstones or pelletal-bioclastic wackestones overlain by ooid grainstones. Judging from the composition of parasequences and thickness relations of their members, the first type is interpreted to comprise late transgressive system tract (ITST) and/or early highstand system tract (eHST), while the second type corresponds to a late highstand system tract (1HST) and/or early lowstand system tract (eLST) of a third-order sequence.
Similar content being viewed by others
References
Bahun, S. (1962): Geoloski odnosi okolice Donjeg Pazaristau u Lici. —M. Sci. Thesis, University of Zagreb, Faculty of Science, 1–36, Zagreb
Buonocunto, F.P., D'Argenio, B., Ferreri, V. and Raspini, A. (1994): Microstratigraphy of highly organized carbonate platform deposits of Cretaceous age. The case of Serra Sbregavitelli Matese (Central Apennines).—Giornale Geol. 56, 179–192, Bologna.
Cosovic, V. (1987): Biostratigraphic features of Jurassic sediments in Gorski Kotar.—Chem. Soc. Geol. Ital.40, 85–89, Roma
D'Argenio, B., Ferreri, V., Ardillo, F. and Buonocunto, F.P. (1993): Microstratigrafia e stratigrafia sequenziale. Studi sui depositi di piattaforma carbonatica, Cretacico del Monte Maggiore (Appennino Meridionale).—Boll. Soc. Geol. Ital.112, 739–749, Roma.
D'Argenio, B., Ferreri, V., Amodio S. and Pelosi, N. (1997): Hierarchy of high-frequency orbital cycles in Cretaceous carbonate platform strata.—Sedimentary Geology113, 169–193, Amsterdam
Egenhoff, S.O., Peterhänsel, A., Bechstädt, T., Zühlke, R. and Grötsch, J. (1999): Facies architecture of an isolated carbonate platform: tracing the cycles of the Latemar (Middle Triassic, northern Italy).—Sedimentology46, 893–912, Oxford
Flügel, E. (1982). Microfacies Analysis of Limestones.—1–636, Berlin (Springer)
Goldhammer, R.K., Oswald, E.J. and Dunn, P.A. (1990): Forward modeling of high-frequency, depositional sequences: an example from Middle Pennsylvanian shelf carbonates of the SW Paradox Basin, Honnacker Trail, Utah.—Abstr. Am. Assoc. Petrol. Geol. Bull.74, 663, Tulsa
Goldhammer, R.K., Dunn, P.A. and Hardie, L.A. (1990): Depositional cycles, composite sea-level changes, cycle stacking patterns, and the hierarchy of stratigraphic forcing: examples from Alpine Triassic platform carbonates.—Geol. Soc. Am. Bull.102, 525–562, Boulder
Gonzales, R. (1996): Response of shallow-marine carbonate facies to third-order and high-frequency sea-level fluctuations: Hauptrogenstein Formation, northern Switzerland.—Sedimentary Geology102, 111–130, Amsterdam
Gusic, I. (1969): Biostratigraphic and micropaleontologic characteristics of some Jurassic cross-sections in Central Croatia.— Geol. Vjesnik22, 89–97, Zagreb
Gusic, I. and Babic, Lj. (1970). Neke biostratigrafske i litogenetske osobine jure Zumberka.—Geol. Vjesnik23, 39–56, Zagreb
Gusic, I. and Jelaska, V. (1990): Upper Cretaceous stratigraphy of the Island of Brac within the geodynamic evolution of the Adriatic carbonate platform.—Opera Acad. Scient. Art Slav. Meridional69, 1–160, Zagreb
— and— (1990): Upper Cenomaian-Lower Turonian sea-level rise and its consequences on the Adriatic-Dinaric carbonate platform.—Geol. Rundschau82/4, 676–68, Berlin
Gusic, I., Nikler, L. and Sokac, B. (1971): The Jurassic in the Dinaric mountains of Croatia and the problems of ist subdivision.— Ann. Inst. Geol. Publ. Hung.54/2, 165–183, Budapest
Hallock, P. (1981): Production of carbonate sediments by selected large benthic foraminifera on two Pacific coral reefs.—J. Sedim. Petrol.51, 467–471, Tulsa
Herak, M. (1968): Noviji rezultati istrazivanja osnovnih stratigrafskih jedinica u Zumberku.—Geol. Vjesnik21, 111–116, Zagreb
— (1986): A new concept of geotectonics of the Dinarides.—Acta Geologica16/1, 1–42, Zagreb
Herak, M., Majcen, Z. and Korolija, B. (1965): Prilog paleontoloskoj dokumentaciji mezozoika u Samoborskom gorjui, sjeveroistocnom Zumberku.—Geol. Vjesnik18/2, 325–331, Zagreb
Jelaska, V. (1971): Korelacija karbonatnog lijasa Dinarida u podrucju Hrvatske i Slovenije.—M. Sci. Thesis, University of Zagreb, Faculty of Science, 1–47, Zagreb
Jelaska, V., Gusic, I., Jurkovsek, B., Ogorelec, B., Cosovic, V., Sribar, L. and Toman, M. (1994): The Upper Cretaceous geodynamics evolution of the Adriatic-Dinaric carbonate platform(s).—Géologie Méditerranéenne21/3–4, 89–91, Marseille
Jelaska, V., Bencek, D., Maticec, D., Belak, M. and Gusic, I. (2000): Geological History and Structural Evolution of the Outer Dinarides.—In: Vlahovic, I. and Biondic, R. (eds.): Second Croatian Geological Congress, Excursion Guide-Book 1–12, Zagreb
Jenkyns, H.C. (1991): Impact of Cretaceous sea level rise and anoxic events in the Mesozoic carbonate platform of Yugoslavia.— Am. Assoc. Petrol. Geol. Bull.75, 1007–1017, Tulsa
Kamp, P.J.J. and Naish, T. (1998): Forward modelling of the sequence stratigraphic architecture of shelf cyclothems: application to Late Pliocene sequences, Wanganui Basin (New Zealand).—Sedimentary Geology116, 57–80, Amsterdam
Kendall, C.G.St.C. and Schlager, W. (1981): Carbonates and relative changes in sea level.—Marine Geology44, 181–212, Amsterdam.
Koerschner III, W.F. and Read, J.F. (1989): Field and modelling studies of Cambrian carbonate cycles, Virginia Appalachians.— J. Sedim. Petrol.59, 654–687, Tulsa
Mitchum, R.M. and Van Wagoner, J.C. (1991): High-frequency sequences and their stacking patterns: sequence-stratigraphic evidence of high-frequency eustatic cycles.—Sedimentary Geology70, 131–160, Amsterdam
Muti, M. (1994): Association of tepees and paleokarst in the Ladinian Calcare Rosso (Southern Alps, Italy).—Sedimentology41, 621–641, Oxford
Nikler, L. and Sokac, B. (1968): Biostratigraphy of the Jurassic of Velebit (Croatia).—Geol. Vjesnik21, 161–176, Zagreb
Pamic, J., Gusic, I. and Jelaska, V. (1998): Geodynamic evolution of the Central Dinarides.—Tectonophysics297, 251–268, Amsterdam
Polsak, A., Bauer, V. and Sliskovic, T. (1982): Stratigraphie du Crétacé Supérieur de la Plate-forme Carbonatée dans les Dinarides Externes.—Cretaceous Res.3, 125–133, London
Radoicic, R. (1966): Microfaciès du Jurassique des Dinarides externes de la Youngoslavie.—Geologija9,5–378, Ljabljana
Rafaelli, P., Scavnicar, B. and Simunic, A. (1965): Petrografske karakteristike nekih karbonatnih stijenajure Velebita, Gorskog kotara i donjeg toka Korane.—Geol. Vjesnik18/2, 245–253, Zagreb
Read, J.P., Grotzinger, J.P., Bova, J.A. and Koerschner, W.-F. (1986): Models for generation of carbonate cycles.—Geology14, 107–110, Boulder
Savic, D. (1972): Razyoj jure i krede izmedu Gornjeg Jelenja i Grobnickog polja.—Geol. Vjesnik25, 127–148, Zagreb
Schlager, W. (1992): Sedimentology and sequence stratigraphy of reefs and carbonate platforms.—Amer. Assoc. Petrol. Geol., Contin. Educ. Course Note Ser.34, Tulsa
Simone, L. (1980): Ooids: A review.—Earth-Sci. Rev.16, 319–355, Amsterdam
Slos, L.L. (1963): Sequences in the cratonic interior of North America.—Geol. Soc. Am. Bull.74, 93–114, Boulder
Slos, L.L., Krumbein, W.C. and Dapples, E.C. (1949): Integrated facies analysis.—In: Longwell, R. (ed.): Sedimentary facies in Geologic History.—Geol. Soc. Am.,39, 91–124, Boulder
Smith, S.V. (1973): Carbon dioxide dynamics: a record of organic carbon production, respiration and calcification in the Enewetak windward reef flat community.—Limnol. Oceanogr.18, 106–120, Canmore
Tucker, M.E. (1993): Carbonate diagenesis and sequence stratigraphy.— In: Wright, V.P. (ed.), Sedimentology Review1, 51–72, Oxford
Tucker, M.E. and Wright, P.V. (1990): Carbonate sedimentology.—1–482, Oxford, (Blackwell)
Vail, P.R., Audemard, F., Bowman, S.A., Eisner, P.N. and Perez-Cruz, C. (1991): The Stratigraphic Signatures of Tectonics, Eustasy and Sedimentology-an Overview.—In: Einsele, G., Ricken, W. and Seilacher, A. (eds.), Cycles and Events in Stratigraphy, 617–659, Berlin (Springer).
Van Wagoner, J.C., Posamentier, H.W., Mitchum, R.M., Vail, P.R., Sarg, J.F., Loutit, T.S. and Hardenbol, J. (1988): An overview of the fundamentals of the sequence stratigraphy and key definitions.—In: Wilgus, C.K., Hastings, B.S., Kendall, C.G.S.C., Posamentier, H.W., Ross, C.A. and Van Wagoner, J.C. (eds.): Sea Level Changes: An Integrated Approach—Soc. Econ. Paleont. Miner., Spec. Publ.,42, 39–45, Tulsa
Velic, I. (1977): Jurassic and Lower Creataceous assemblage zones in Mt. Velika Kapela, Central Croatia.—Acta Geol.9/2, 15–37, Zagreb
Wilson, J.L. (1975): Carbonate facies in geologic history.—1–471, Berlin (Springer).
Author information
Authors and Affiliations
Rights and permissions
About this article
Cite this article
Buckovic, D., Jelaska, V. & Tesovic, B.C. Facies variability in Lower Liassic carbonate successions of the Western Dinarides (Croatia). Facies 44, 151–162 (2001). https://doi.org/10.1007/BF02668172
Received:
Accepted:
Issue Date:
DOI: https://doi.org/10.1007/BF02668172